GeoSwath 2007


WORKSHOPS ANNOUNCEMENT
GeoSwath: Western US

Sponsored by a grant from the National Science Foundation

The GeoSwath initiative, a geologically-inspired EarthScope activity linked to USArray, involves integration of geology and geophysical imaging toward understanding the 4-D construction, stabilization and modification of the North American continent. GeoSwath emphasizes a continuous coast-to-coast perspective that examines fundamental tectonic processes, the continent's major geologic provinces and their boundaries.

Two workshops in 2007 will bring together complementary segments of the U.S. geoscience community, including geologists, geophysicists and geochronologists.

  1. The topic of the first workshop, co-sponsored by MARGINS, is the connection between the US continental interior and its western plate margin. Thus, it focuses on the two westernmost GeoSwath target areas, which are the Walker Lane belt and Cascadia. It will be held on March 27, prior to the 2nd National EarthScope meeting in Monterey (CA). Go to http://www.nsf-margins.org/Geoswath07 for application information; the deadline is February 15.
  2. The second workshop, co-sponsored by IRIS, will focus on integrated continental science in a continuous swath extending from the Pacific northwest coast to the Great Plains between 42-47° N latitude. Thus, it covers the 'Lewis and Clark' or Western GeoSwath that includes the Cascadia, Northern Rockies and Black Hills/Great Plains target areas. It will be held on April 27-29 in Boise, ID. Go to http://www.globalchange.umich.edu/ben/geoswath/ for application information; the deadline is March 1.

GeoSwath funding will partially support the costs of housing, food and a contribution toward the travel of participants. For more information, please contact Randy Keller (grkeller@ou.edu), Basil Tikoff (basil@geology.wisc.edu), or Ben van der Pluijm (vdpluijm@umich.edu).


Index

Monterey Workshop

March 27, 2007

Description
 


Boise Workshop

April 27 (6pm) to 29 (noon), 2007

Description


(geoswath07@umich.edu)


Extended Description

A full description of the Geologic Framework for EarthScope's USArrray that led to the concept of GeoSwath was published in EOS, v. 87, p. 221/224. The figure below is reproduced from this article.


(from Tikoff et al.,  EOS, 87, 221/224)

 

The EarthScope Project has the potential to be a transformative activity for the geosciences and to take the solid Earth sciences a step beyond plate tectonics, but only if structural geology, sedimentology, petrology, geochronology, geochemistry, and geophysics are combined in an integrated manner to study the structure and evolution of the lithosphere. A goal of the GeoSwath initiative is to help accomplish this task by focusing on the 4-D construction, stabilization and modification of the North American continent, through integration of geology and geophysical imaging under EarthScope. This initiative encourages a cooperative community approach to collecting and sharing data, and takes a connected, coast-to-coast perspective that examines fundamental processes, the continent’s major geologic provinces and their boundaries. This approach requires the contribution of large segments of the U.S. geosciences community, particularly those who provide the crucial information about Earth history across both space and time.

 

At its initial workshop, seven focus regions across the conterminous United States were identified (see EOS, 87, 221/224), and additional community input has been received during Town Hall meetings held during the Geological Society of America and American Geophysical Union national meetings held during the fall of 2006. Now our goal is to bring the community together to formulate a science plan and produce research partnerships that will result in specific proposals. Thus two workshops will be held early in 2007.

 

The first workshop is co-sponsored by MARGINS and is linked to the national EarthScope meeting in March in Monterey, CA. This workshop will focus on the two westernmost target areas of the GeoSwath initiative, which are the Walker Lane belt and Cascadia.

Walker Lane: The Walker Lane Belt, situated in the western Basin and Range province, will seamlessly integrate surface geology, topography, and the history of the continental lithosphere with ongoing processes in the Earth’s mantle. Specifically, the area allows study of the present modification of continental lithosphere by the process of transform faulting and rifting. Studies here will leverage the NSF Margins initiative in the Gulf of California by extending the scientific investigations onshore from the Gulf of California to the north into Nevada.

 

Cascadia: The Pacific Northwest offers the best place in the conterminous United States to investigate an active subduction zone, the process of magmatic addition to the continental crust (Cascadia arc, High Lava Plains, Idaho batholith), and the interaction of deformation and magmatism. This is also potentially the best area in the North American Cordillera to study tectonic accretion and subsequent modification of the lithosphere.

 

The second workshop is co-sponsored by IRIS and will be held April 27-29 in a northern Rockies location. It will focus on integrated continental science in a continuous swath extending from the Pacific northwest coast to the Great Plains between 42-47° N latitude. Thus, it covers the 'Lewis and Clark' or western GeoSwath that includes the Cascadia, Northern Rockies and Black Hills/Great Plains GeoSwath target areas.

 

Northern Rockies: The Northern Rockies have a diverse and extensive geologic history that is recorded in rocks that range from ancient (>3.5 billion years old) gneisses of the Wyoming Craton to the modern Yellowstone hot spot/Snake River Plain. The region provides an opportunity to examine two challenging problems in the study of the formation and evolution of continental crust: (1) how newly segregated, low-density crust and lithosphere are integrated into compositionally and structurally mature continents; and (2) how newly formed crust and lithosphere evolve within the continental environment.

 

Black Hills/Great Plains: The Black Hills is a type locality of intracratonic deformation, allowing investigation of how displacements/stresses are transferred far into the continental interior. Further, there is a clear indication of crustal- and lithospheric-scale reactivation associated with Laramide uplifts (Black Hills, Bighorn Mountains), although the lithospheric signature of these processes is unknown. It is also possible to investigate large-scale uplift of the entire Great Plains and its possible lithospheric causes.

 

Together, the Cascadia, Northern Rockies and Black Hills/Great Plains target areas constitute the ‘Lewis and Clark’ or western swath. The sum of these three areas will allow the examination of modern continental tectonics and the ongoing formation of a mountain belt, and provide a balanced cross section across an entire orogenic belt from hinterland to extended foreland.

 


Monterey workshop

March 27, 2007.

Go to: http://www.nsf-margins.org/Geoswath07/

 

 


Boise workshop

April 27-29, 2007.

Allen Richard M. UC- Berkely
Barnes Calvin Texas Tech
Benford Bryn Wisconsin
Braile Lawrence W. Purdue Univ.
Chamberlain Kevin R. University of Wyoming
Cummings Michael  Portland State University
Dorsey Rebecca J.  University of Oregon
Dueker Ken  University of Wyoming
Duke Edward F. South Dakota School of Mines & Tech
Erslev Eric  Colorado State
Foster David Univ. Flordia
Fuis Gary USGS
Gao Stephen S. University of Missouri
Glenn Nancy Idaho State University
Harlan Stephen S.  George Mason University
Hole John Virgina Tech
Housen Bernie  Western Washington University
Ingate Shane F.  IRIS
Janecke Susanne Utah State University
Keller Randy Oklahoma
Lageson Dave Montana State University
Lewis Reed  Idaho Geologic Survey and Univ. of Idaho 
Link Paul  Idaho State University
Lisenbee Alvis L.  South Dakota School of Mines & Tech
Lowry Tony Utah State University
Lund Karen USGS
Mahan Kevin R. Cal-Tech
Manduca Cathryn A. Carlton College
Mickus Ken  Missouri State
Mogk David W.  Montana State University
Mueller Paul A.  Univ. Flordia
Northrup C. J.  Boise State
Okure Maxwell Oklahoma
Oldow John S.  Univ. Idaho
Rodgers David Idaho State University
Russo Ray  Univ. Flordia
Schmitz Mark Boise State
Schnyder Walt Boise State
Shaw Colin Montana
Shervais John Utah State University
Siddoway Christine  Colorado College
Smaltz Sara Colorado State
Smith Bob Utah
Snelson Cathy UNLV
Terry Michael  South Dakota School of Mines & Tech
Tikoff Basil Wisconsin
van der Pluijm Ben Michigan
Vervoort Jeff  Washington State University
Yuan Huaiyu University of Wyoming

 

SpringHill Suites by Marriott

http://marriott.com/property/propertypage/BOIDT

424 East Parkcenter Blvd

Boise, ID 83706

ph: 208-342-1044

Airport-Hotel transportation is available.

 

Start: Friday, April 27 at 6pm (reception and dinner+speaker)

End: Sunday, April 29 at noon

 

 

 

 

 

 

 

 

Application CLOSED

Email your interest to participate in the Boise GeoSwath workshop to: geoswath07@umich.edu (this reaches Ben van der Pluijm and Sara Tourscher).


Include in your email

Faculty, research scientists, post-doctoral fellow and senior PhD students are all encouraged to attend. 
We will decide by mid-March on participation, allowing sufficient time for travel planning to Boise.

 

We will support all lodging and meals for the workshop and make a significant contribution toward your travel.  Local arrangements have already been made, based on shared lodging (large suites!).  Transportation arrangements to Boise are your own responsibility.  Plane, bus, car, bike, foot are all allowed. 

 

Please make sure that you are available for the duration of the workshop, from Friday's reception/dinner to Sunday noon (no lunch planned to allow convenient departure times).

 

Contact us for more info, Randy Keller (grkeller@ou.edu ), Basil Tikoff (basil@geology.wisc.edu ), Ben van der Pluijm (vdpluijm@umich.edu ), or use our GeoSwath07 email address above.
 

 


December 21, 2007.